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Figure 5 | Earth, Planets and Space

Figure 5

From: Velocity increase in the uppermost oceanic crust of subducting Philippine Sea plate beneath the Kanto region due to dehydration inferred from high-frequency trapped P waves

Figure 5

Assumed P -wave velocity structure and simulation results of the JIVSM. (a) 2D P-wave velocity structure assumed by the JIVSM. (b) Snapshots of the seismic wave propagation at lapse times of t = 7 and 14 s. (c) Simulated vertical velocity seismograms at station N.NSHH (111 km). The star and filled triangles in (a) are the location of the hypocenter and seismic station (N.NSHH), respectively. The dashed and solid lines in (c) are the onsets of the P and trapped P waves, respectively.

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